Suitable areas for subirrigation and sprinkler irrigation were identified in Richelieu and St-Hyacinthe counties. / Land suitable for subirrigation includes uniform sandy textured profiles deeper than 1 m, with hydraulic conductivities greater than 0.5 m/d and lying on a clay layer at approximately 2 m from the surface, and with slopes less than 0.5% and little or no microrelief. / Soils that failed to satisfy the subirrigation criteria and that would most benefit from sprinkler irrigation were identified. These soils had available water holding capacities of less than 7.5 cm per 100 cm of soil. Most of the soils suitable for sprinkler irrigation were shallow sand (50 cm) over clay. / Both the Richelieu and St-Lawrence Rivers could meet the flow demand for the total irrigated area. However, 57% of the subirrigable land is located at more than 20 km from the Richelieu and St-Lawrence and could be more economically supplied by the Yamaska River. The Yamaska River could supply all the subirrigated land in its vicinity (4 900 ha) and part of the land suited for sprinkler irrigation (1 000 ha) 4 out of 5 years. (Abstract shortened by UMI.)

Field water table measurements were taken at two sites in Southern Quebec in order to validate DRAINMOD, a field scale water table management model. Two growing seasons of data were collected on a loamy sand soil near Sorel, Quebec and one year of data on a clay soil to the south-west of Montreal. Several water table management schemes were investigated, ranging from conventional subsurface drainage to automated subsurface irrigation. / DRAINMOD was used to simulate the measured water table fluctuations and relative corn crop yields over the growing season. Verification of the model was needed to determine if it could be a useful tool in the design and operation of water table management systems for the Quebec region. / It was found that DRAINMOD output closely simulated the water table fluctuations for conventional drainage and subsurface irrigation plots provided no exceptional circumstances existed. More study is needed in some areas such as bedded fields and in the use of fluctuating water level control structures.

Thesis (M.Sc.)--Victoria University of Wellington, 2008. / Includes bibliographical references.

A grande quantidade de resíduos sólidos gerados nas cidades é um desafio para o saneamento ambiental no Brasil. A fim de se reduzir os impactos gerados ao meio ambiente e à saúde pública, é necessário que haja um gerenciamento adequado, desde a coleta até a disposição final, desses resíduos sólidos urbanos. Os aterros sanitários permitem um maior controle ambiental, desde que sejam bem projetados e operados. A decomposição da matéria orgânica presente nesses resíduos, somada às águas das chuvas gera o lixiviado, líquido com alto potencial poluidor. Várias formas de tratamento são propostas com a finalidade de tornar o lixiviado menos poluente ao meio ambiente. Wetlands construídos tem se mostrado uma alternativa eficiente para a remoção de poluentes em lixiviados, além dos baixos custos operacionais e de implantação. O presente estudo investigou o uso de wetlands subsuperficiais em escala-piloto para o tratamento de um lixiviado prétratado. Os wetlands foram monitorados com a finalidade de se obter remoções de matéria orgânica e nitrogênio amoniacal. As maiores reduções percentuais de concentração de nitrogênio amoniacal, DQO e COD foram, 91%, 42% e 35%, respectivamente. As maiores reduções percentuais em carga de nitrogênio amoniacal e DQO foram, 67% e 50%, respectivamente. Os resultados dos ensaios de toxicidade realizados com os organismos Vibrio fischeri e Danio rerio revelaram que, a toxicidade do lixiviado foi reduzida ao ser tratado pelo wetland. / Large amounts of solid wastes are generated in cities and this is a challenge for environmental sanitation in Brazil. In order to reduce impacts to the environment and to public health, it is necessary to manage these municipal solid wastes appropriately, from their collection to their final disposal. Landfills allow a greater environmental control, provided that they are well designed and operated. Landfill leachate generation results from the decomposition of the organic matter in the wastes, combined with the rainwater that percolates the waste. Landfill leachate has a high pollution potential. Various forms of treatment are proposed in order to attenuate the potential of the leachate to pollute the environment. Constructed wetlands seem to be efficient alternatives in removing leachate pollutants with low operational and implementation costs. The present study investigated the use of subsurface wetlands in pilot scale in a pretreated leachate treatment. The wetlands were monitored in order to obtain results in reducing the concentration and loads of pollutants. The best removal performance of the concentration of ammonia nitrogen, COD and DOC were 91%, 42% and 35%, respectively. The best removal performance of the load of ammonia nitrogen and DOC were 67% and 50%, respectively. The results of the toxicity tests conducted with Vibrio fischeri and Danio rerio revealed that wetlands were effective in reducing the toxicity of the leachate.

This study utilises seismic data to improve understanding of the subsurface fluid flow behaviour in the Taranaki and Great South Basins offshore New Zealand. The aim of this study is to characterise fluid flow features and to investigate their genesis, fluid origins and implications for subsurface fluid plumbing system by integrating seismic interpretation and 3D petroleum systems modelling techniques. After an early phase studying Pliocene pockmarks in the Taranaki Basin, this study has been focused on the subsurface fluid plumbing system and on the fluid expulsion history in the Great South Basin. The Taranaki Basin lies on the west coast and offshore of the North Island, New Zealand. The seismic interpretation revealed that paleo-pockmark formation in the study area relates to fluid escape due to a rapid sediment loading environment in a distal fan setting. Seismic analysis rules out any links between the paleo-pockmarks and faulting. The relationship between paleo-pockmark occurrence and fan depositional thickness variations suggests that pore-water expulsion during overburden progradation is the most likely cause of the paleo-pockmarks. The rapid sediment loading generated overpressure which was greatest on the proximal fan due to a lateral gradient in overburden pressure. Fluids were consequently forced towards the fan distal parts where, eventually, the pore pressure exceeded the fracture gradient of the seal. The Great South Basin lies off the southern coast of the South Island of New Zealand and is located beneath the modern shelf area. Evidence for past and present subsurface fluid flow in this basin is manifested by the presence of numerous paleo-pockmarks, seabed pockmarks, polygonal fault systems, bright spots and bottom simulating reflections (BSR), all of which help constrain aspects of the overburden plumbing system and may provide clues to deeper hydrocarbon prospectivity in this frontier region. The various types of fluid flow features observed in this study are interpreted to be caused by different fluid origins and mechanisms based on evidences from seismic interpretation in the study area. The possible fluid origins which contribute to fluid flow features in the Great South Basin are compactional pore water as well as biogenic and thermogenic hydrocarbons. Using 3D seismic attribute analysis it was possible to highlight the occurrence of these features, particularly polygonal faults and pockmarks, which tend to be hosted within fine-grained sequences. Paleo- and present-day fluid flow features were investigated using 3D basin and petroleum systems modelling with varying heat flow scenarios. The models predict that thermogenic gas is currently being generated in mid-Cretaceous sedimentary sequences and possibly migrates along tectonic faults and polygonal faults feeding present-day pockmarks at the seabed. The models suggest that biogenic gas was the main fluid source for the Middle Eocene paleo-pockmarks and compactional pore fluid may be the main fluid contributor to the Late Eocene paleo-pockmarks. Different heat flow scenarios show that only mid-Cretaceous source rocks have reached thermal maturity in the basin, whilst Late Cretaceous and Paleocene source rocks would be largely immature. The observations and interpretations provided here contribute to the ongoing discussion on basin de-watering and de-gassing and the fluid contributors involved in pockmark formation and the use of pockmarks as a potential indicator of hydrocarbon expulsion. It is clear from this study that seismically-defined fluid flow features should be integrated into petroleum systems modelling of frontier and mature exploration areas in order to improve our understanding on fluid phases, their migration routes, timings and eventual expulsion history.

A grande quantidade de resíduos sólidos gerados nas cidades é um desafio para o saneamento ambiental no Brasil. A fim de se reduzir os impactos gerados ao meio ambiente e à saúde pública, é necessário que haja um gerenciamento adequado, desde a coleta até a disposição final, desses resíduos sólidos urbanos. Os aterros sanitários permitem um maior controle ambiental, desde que sejam bem projetados e operados. A decomposição da matéria orgânica presente nesses resíduos, somada às águas das chuvas gera o lixiviado, líquido com alto potencial poluidor. Várias formas de tratamento são propostas com a finalidade de tornar o lixiviado menos poluente ao meio ambiente. Wetlands construídos tem se mostrado uma alternativa eficiente para a remoção de poluentes em lixiviados, além dos baixos custos operacionais e de implantação. O presente estudo investigou o uso de wetlands subsuperficiais em escala-piloto para o tratamento de um lixiviado prétratado. Os wetlands foram monitorados com a finalidade de se obter remoções de matéria orgânica e nitrogênio amoniacal. As maiores reduções percentuais de concentração de nitrogênio amoniacal, DQO e COD foram, 91%, 42% e 35%, respectivamente. As maiores reduções percentuais em carga de nitrogênio amoniacal e DQO foram, 67% e 50%, respectivamente. Os resultados dos ensaios de toxicidade realizados com os organismos Vibrio fischeri e Danio rerio revelaram que, a toxicidade do lixiviado foi reduzida ao ser tratado pelo wetland. / Large amounts of solid wastes are generated in cities and this is a challenge for environmental sanitation in Brazil. In order to reduce impacts to the environment and to public health, it is necessary to manage these municipal solid wastes appropriately, from their collection to their final disposal. Landfills allow a greater environmental control, provided that they are well designed and operated. Landfill leachate generation results from the decomposition of the organic matter in the wastes, combined with the rainwater that percolates the waste. Landfill leachate has a high pollution potential. Various forms of treatment are proposed in order to attenuate the potential of the leachate to pollute the environment. Constructed wetlands seem to be efficient alternatives in removing leachate pollutants with low operational and implementation costs. The present study investigated the use of subsurface wetlands in pilot scale in a pretreated leachate treatment. The wetlands were monitored in order to obtain results in reducing the concentration and loads of pollutants. The best removal performance of the concentration of ammonia nitrogen, COD and DOC were 91%, 42% and 35%, respectively. The best removal performance of the load of ammonia nitrogen and DOC were 67% and 50%, respectively. The results of the toxicity tests conducted with Vibrio fischeri and Danio rerio revealed that wetlands were effective in reducing the toxicity of the leachate.

Magister Scientiae - MSc (Environ & Water Science) / Studies have shown that the primary origin of salinity in river flows of the Sandspruit in the Berg Catchment located in the Western Cape Province of South Africa was mainly a result of atmospheric deposition of salts. The salts are transported to rivers through surface runoff and subsurface flow (i.e. through flow and groundwater flow). The purpose of this study was to determine the contributions of subsurface and surface flows to the total flows in the Sandspruit, Berg Catchment. Three rain events were studied. Water samples for two rain events were analysed for environmental tracers ?18O, Silica or Silicon dioxide (SiO2), Calcium (Ca2+) and Magnesium (Mg2+). Tracers used for two component hydrograph separation were ?18O and SiO2. The tracers, Ca2+ and Mg2+, revealed inconsistent contributions of both subsurface flow and surface flow. Two component hydrograph separations indicated is that groundwater is the dominant contributor to flow, while surface runoff mainly contributes during the onset of the storm event. Groundwater response to precipitation input indicated that boreholes near the river have a quicker response than boreholes further away from the river. Boreholes nearer to the river also indicate higher water levels in response to precipitation, in comparison to boreholes further from the river.

Magister Scientiae - MSc (Environ & Water Science) / Studies have shown that the primary origin of salinity in river flows of the Sandspruit in the Berg Catchment located in the Western Cape Province of South Africa was mainly a result of atmospheric deposition of salts. The salts are transported to rivers through surface runoff and subsurface flow (i.e. through flow and groundwater flow). The purpose of this study was to determine the contributions of subsurface and surface flows to the total flows in the Sandspruit, Berg Catchment. Three rain events were studied. Water samples for two rain events were analysed for environmental tracers ?18O, Silica or Silicon dioxide (SiO2), Calcium (Ca2+) and Magnesium (Mg2+). Tracers used for two component hydrograph separation were ?18O and SiO2. The tracers, Ca2+ and Mg2+, revealed inconsistent contributions of both subsurface flow and surface flow. Two component hydrograph separations indicated is that groundwater is the dominant contributor to flow, while surface runoff mainly contributes during the onset of the storm event. Groundwater response to precipitation input indicated that boreholes near the river have a quicker response than boreholes further away from the river. Boreholes nearer to the river also indicate higher water levels in response to precipitation, in comparison to boreholes further from the river.

Doctor of Philosophy / Department of Biological & Agricultural Engineering / Aleksey Y. Sheshukov / As the world faces an increasing demand for food due to the growing global population and the pernicious effects of land degradation, there is a need to overcome this challenge by using sustainable management practices for agricultural productions. One of the problems, which sustainable agriculture seeks to address, is the loss of topsoil due to soil erosion. Changing weather patterns also contribute to the average annual rainfall across the globe with an excess precipitation, which creates runoff and causes soil erosion. One of the significant yet less studied types of soil erosion is ephemeral gully erosion. Formed by the concentrated overland flow during intensive rainfall events, ephemeral gullies are channels on agricultural fields that can be removed by tillage operations but appear at the same location every year. Even though simplified ephemeral gully models estimate soil losses, they do not account for complicated hydrological and soil erosion processes of channel formations. The purpose of this research work is to investigate sediment sources and develop tools that can predict ephemeral gully erosion more efficiently. To achieve this goal, an experimental study was conducted on an agricultural field in central Kansas by tracking channel development, monitoring soil moisture content, and recording the amount of rainfall. Runoff and sediment loads from contributing catchment and critical and actual shear stresses were estimated by the computer model, and conclusions were made on the effect of saturation dynamics on the erosion processes. Furthermore, a two-dimensional subsurface water flow and soil erosion model was developed with the variable soil erodibility parameters which account for the subsurface fluxes and the effects on the soil detachment process. The model was applied to study the impacts of variable soil erodibility parameters on the erosion process for different soils and various antecedent soil moisture conditions. Also developed to estimate the soil losses at the field scale was an integrated spatially-distributed ephemeral gully model with dynamic time-dependent channel development. The model showed good fit by matching the experimental data. The results from this work can be used to advance the research of soil erosion prediction from concentrated flow channels and ephemeral gullies formed on agricultural fields.

Made available in DSpace on 2014-06-11T19:23:11Z (GMT). No. of bitstreams: 0 Previous issue date: 2011-06-20Bitstream added on 2014-06-13T19:29:02Z : No. of bitstreams: 1 ramos_sb_me_jabo.pdf: 678005 bytes, checksum: c26818a4aa88fbc25a2c9fa8ae65fb8f (MD5) / Embora o gesso agrícola seja um insumo utilizado na cultura da cana-de-açúcar, em praticamente todas as regiões produtoras do País, persistem ainda algumas dúvidas sobre os benefícios proporcionados por sua aplicação. O trabalho objetivou avaliar doses de gesso agrícola nos atributos químicos do solo, na densidade de matéria seca de raiz, na produtividade e qualidade tecnológica da cultura por duas safras consecutivas. O experimento foi instalado em Dracena, SP, com delineamento em blocos casualizados, com quatro repetições, em parcelas sub-subdivididas para atributos químicos do solo e subdivididas para densidade de matéria seca de raiz, qualidade tecnológica e produtividade, tendo como tratamentos, doses de gesso (0, 1, 2, 4 e 8 t ha-1) aplicadas após o terceiro corte da cana, períodos de avaliação (Anos agrícolas 2007/08 e 2008/09) e profundidade de amostragem (0-0,2; 0,2-0,4; 0,4-0,6; 0,6-0,8 e 0,8-1,0 m), em um Latossolo Vermelho-Amarelo distrófico, de textura média. Foram coletadas amostras de solo nas mesmas camadas, antes da instalação do experimento e depois de cada colheita. No segundo ano agrícola foi avaliada a densidade de matéria seca de raiz. As análises químicas de solo identificaram aumentos de Ca, S e saturação por bases e redução da saturação por alumínio. A aplicação do gesso agrícola promoveu a movimentação do Mg no primeiro ano agrícola, porém não foi observada a lixiviação do K. O gesso agrícola aumentou significativamente a densidade de matéria seca de raiz. Os tratamentos com doses de gesso não alteraram significativamente a ATR e produtividade da cana-de-açúcar / Although agricultural gypsum is an input used in the sugar cane crop in practically all producing regions in the country, there are still some questions regarding the benefits provided through its application. The purpose of this study was to evaluate the effect of rates of agricultural gypsum on soil chemical attributes, on root dry matter density, and on the yield and technological quality of the crop throughout two consecutive crop seasons. The experiment was carried out in Dracena, SP with a randomized block design with four replications in split-split plots for soil chemical attributes and split plots for root dry matter density, technological quality and yield, with treatments being rates of gypsum (0, 1, 2, 4 and 8 t ha-1) applied after the third cutting of the sugar cane, periods of assessment (2007/08 and 2008/09 crop seasons) and depth of sampling (0-0.2; 0.2-0.4; 0.4-0.6; 0.6-0.8 and 0.8-1.0 m), in a Haplustox soil. Soil samples were collected at the same layers before carrying out the experiment and after each harvest. In the second crop season, the root dry matter density was assessed. Soil chemical analyses identified increases of Ca, S and base saturation, and reduction of aluminum saturation. Agricultural gypsum application led to leaching of Mg in the first crop year, however, leaching of K was not observed. Agricultural gypsum significantly increased root dry matter density. Treatments with rates of gypsum did not significantly modify the Total Recoverable Sugar (TRS) and sugar cane yield